作者: V.J. Allison , L.M. Condron , D.A. Peltzer , S.J. Richardson , B.L. Turner
DOI: 10.1016/J.SOILBIO.2007.02.006
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摘要: During primary succession, the abundance of carbon (C) and nitrogen (N) in soil increases, while phosphorus (P) declines. These changes in nutrient concentrations in organic matter are likely to play an important role in controlling enzyme-mediated nutrient mineralization. We examined how enzyme activity and efficiency changed with successional time in organic and mineral soils taken from the 120000-year-old Franz Josef soil development sequence, New Zealand, and the relationship between enzyme activity and efficiency and soil nutrient …